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  • 1
    Publication Date: 1970-06-01
    Description: The effect of continuous freezing at −15 C and alternate freezing and thawing on some chemical properties of three Saskatchewan soils was determined. The results are based on soils treated while moist with methyl bromide and freeze-dried following the frost treatments. The freezing effects were obtained by comparisons with air-dried control samples. Alternate freezing and thawing resulted in a large increase in exchangeable NH4-N and a small but significant decrease in exchangeable K; there was no effect on cation exchange capacity or exchangeable Ca++ and Mg++. Freezing and thawing did not affect NO3-N content. Dilute NaHCO3-extractable N and water-soluble carbohydrates, as indices of available N, increased sharply after continuous freezing, but alternate freezing and thawing gave a further increase in NaHCO3-extractable N only in one soil. There was an increase in NaHCO3-extractable P after continuous freezing and a further significant increase following alternate freezing and thawing. The large increase in exchangeable NH4-N as a result of alternate freezing and thawing was not reflected in an increase in N uptake by barley seedlings grown on the frost treated soils. Generally there was good agreement between N uptake and available N results. The uptake of P by the barley seedlings did not reflect the increase in NaHCO3-extractable P as a result of the frost treatments.
    Print ISSN: 0008-4271
    Electronic ISSN: 1918-1841
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
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  • 2
    Publication Date: 1962-08-01
    Description: Pre-weighed monocalcium phosphate pellets, containing about 15 milligrams of P, were placed in 200 grams of soil and stored for 2 weeks at four moisture tensions and three temperatures. Pellet residues were then removed and the amount of phosphorus remaining was determined. Small cores containing pellet residues and the surrounding soil contacted by fertilizer solution were removed for determination of water-soluble and total inorganic P. Phosphate phases present at the granule sites and the surrounding soil were identified by their optical properties.The mean amount of phosphorus remaining at the granule sites was 20.2 per cent. Although both moisture tension and temperature significantly affected the quantity of phosphorus retained, no consistent trend was apparent. Residues remaining at the site of application were found to be mixtures of anhydrous and dihydrated dicalcium phosphate, with the latter predominating. Moisture tension and temperature did not greatly alter the proportion of the two phases.Periodic precipitates or Liesegang rings of dicalcium phosphate were formed in the soil surrounding monocalcium phosphate pellets. Dicalcium phosphate dihydrate was the predominant phase. The proportion of dihydrated to anhydrous dicalcium phosphate increased as the temperature decreased and as the moisture tension increased.Water-soluble P increased significantly with increased moisture tension and was significantly greater at 5 °C. than at either 16 or 27 °C. The mean of all treatments was 5.6 per cent. Increased amounts of dicalcium phosphate dihydrate in the surrounding soil seemed to be responsible for the increase in water solubility.Between 89.5 and 99.2 per cent of the added phosphorus was recovered in the water and acid extracts of soil cores containing about 1.4 cm.3 of soil.
    Print ISSN: 0008-4271
    Electronic ISSN: 1918-1841
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
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  • 3
    Publication Date: 1964-02-01
    Description: Nitrogen, as fixed ammonium, occurred in the five profiles of arable soil of different texture which were examined. The amounts observed increased with increasing soil depth in four of the profiles. Total amounts found in the 4-ft profiles varied from 2600 to 4600 lb per acre and ranged from 7% of the total nitrogen in the surface soil to as much as 58% in the soil at the 4-ft depth.When the fixed ammonium nitrogen was subtracted from the total nitrogen the C:N ratios of these soils increased very sharply with depth, indicating that the subsoil organic matter was less rich in nitrogenous substances than was that of the surface soil.The clay fractions of the profiles were mineralogically similar and contained essentially the same amounts of fixed ammonium, approximately 2.4 meq ammonium per 100 g of clay. The silt fractions contained approximately 1.8 meq fixed ammonium per 100 g of silt. These fractions accounted for nearly all the fixed ammonium nitrogen observed except in the coarser-textured soils.Fixed ammonium and total nitrogen analysis of 25 paired samples of cultivated and virgin soil indicated that although the average total nitrogen had been reduced by one-third, there had been little or no effect on the amount of fixed ammonium N in the surface soil.
    Print ISSN: 0008-4271
    Electronic ISSN: 1918-1841
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
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  • 4
    Publication Date: 1967-02-01
    Description: Wheat was grown in a loam soil that had been treated with N serve, a nitrification inhibitor, and dressed with N and P fertilizers.With the inhibitor, NH4-N accumulated in the soil but NO3-N accumulated where none was used. Uptake of N was less when nitrification was inhibited but uptake of P was greater.
    Print ISSN: 0008-4271
    Electronic ISSN: 1918-1841
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
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  • 5
    Publication Date: 1966-10-01
    Description: Profile samples from two fine-textured soils were analyzed for native fixed NH4, ammonium-fixing capacity, exchangeable K, and organic matter content. Ammonium fixation decreased with proximity to the surface whereas exchangeable K and organic matter increased. Adding KCl to Sceptre subsoil to increase the exchangeable K decreased NH4 fixation approximately in proportion to the amount of KCl added. Destruction of organic matter prior to NH4 fixation increased the amount of NH4 fixed, the increase being greater the higher the organic matter content of the sample. The decrease in NH4 fixation with proximity to the surface was due to potassium ion and organic matter content.
    Print ISSN: 0008-4271
    Electronic ISSN: 1918-1841
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
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  • 6
    Publication Date: 1974-04-01
    Description: Thatcher wheat was grown in tank-type lysimeters over a 7-yr period to determine the effect of fertilizer, two levels of available water and two cropping systems on the yield and nutrient content of grain and on some soil nutrients. Fertilizer did not change the yield of grain materially under natural rainfall. Added water only increased the yield by one-half and three-quarters of continuous wheat and fallow, respectively. Fertilizer with added water nearly doubled the yield of continuous wheat and increased by one-third the yield from the wheat-fallow rotation. The P content of the grain was not affected by fertilization, but was higher in the treatments to which additional water was applied than in those receiving natural rainfall only. It was also higher in continuous wheat than in fallow wheat. There was an interaction between the N and P uptake ratio and the N content of the grain. Fertilizer or additional water or both increased or decreased the N content, depending upon which way the N or P balance was shifted. Surplus available N not utilized by the crop grown with natural rainfall accumulated as nitrates at lower soil depths, particularly under the wheat-fallow system. All the NO3-N produced where supplemental water or water and fertilizer were applied was utilized and none accumulated. The organic N content of the surface soil increased along with a reduced loss in organic C where water and fertilizer were applied, as compared to the other treatments. Fertilizer application resulted in a sharp increase in NaHCO3 soluble P, particularly following the supplemental water plus fertilizer treatments where an excess of P was supplied with the fertilizer over that removed by the crop. There was an increased demand on soil P where water only was applied, and the soluble P content was appreciably reduced.
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    Electronic ISSN: 1918-1841
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  • 7
    Publication Date: 1963-01-01
    Description: The use of NP fertilizer gave consistent increases in yields of wheat on a loam and a clay soil with low NaHCO3 soluble phosphorus contents. The fertilizer increased crop growth during the early part of the growing season hastened maturity, and increased the amount of stooling and the number of mature heads at harvest time.Fertilized crops on both soils used more moisture than unfertilized crops between seedtime and the heading stage. For the season as a whole, no difference in total moisture use was recorded on loam soils between fertilized and check crops but on clay soil some fertilized crops extracted more subsoil moisture than the unfertilized crops.Under the climatic conditions of these experiments yield responses obtained from fertilizer application did not appear to be directly related to the amount of available moisture at seedtime or to the seasonal precipitation. When increased yields were obtained from the use of fertilizer the fertilized crops used moisture more efficiently.The NP fertilization had little or no effect on the phosphorus content of the grain but did increase the total phosphorus uptake by the crops. The fertilizer treatment increased the protein content of wheat grown on stubble on both the loam and the clay soils and on two of the four crops grown on fallow on the loam soil.
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    Electronic ISSN: 1918-1841
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  • 8
    Publication Date: 1972-10-01
    Description: not available
    Print ISSN: 0008-4271
    Electronic ISSN: 1918-1841
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  • 9
    Publication Date: 1975-05-01
    Description: Multiple regression was used to quantify the relationships between NO3 in surface soil versus several selected environmental variables. Measurements were made on summer-fallowed Wood Mountain loam in the field. The temperatures and moisture conditions measured during one growing season were simulated in the laboratory using three soils. The most important factor influencing NO3 change was wetting and drying. The latter's effect was dependent on the soil moisture content just before the change occurred and/or the temperature during the period of change. Nitrification accounted for 12% of the increases in NO3 in the top 2.5 cm of soil; 88% of the increase resulted from upward movement of NO3-salts into the surface layer of soil as a result of evaporation. Of the NO3 produced by nitrification in the Wood Mountain loam, about 17.4% was credited to temperature effects. Thus only about 2.1% of the NO3 increase in the top 2.5 cm of soil in the field was due to temperature. In the simulation study, 19 C appeared to be a critical temperature above which the rate of nitrification was sufficient to counterbalance NO3 losses resulting from leaching and/or denitrification. The effect of moisture change on NO3 change appeared to be directly proportional to the total C and total N content of the three soils.
    Print ISSN: 0008-4271
    Electronic ISSN: 1918-1841
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
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  • 10
    Publication Date: 1962-08-01
    Description: The effect of phosphate source and soil moisture during the initial soil-fertilizer reaction period on subsequent phosphorus uptake by alfalfa was investigated in a growth chamber. Phosphate-treated soils with moisture adjusted to four different tensions were stored at approximately 18 °C. for 10 weeks. Following this storage interval phosphorus uptake by alfalfa was measured using a short-term technique.Phosphorus content and phosphorus uptake by both tops and roots increased significantly when water-soluble materials such as ammonium polyphosphate, monoammonium and monocalcium phosphate were applied. Less soluble sources, i.e., hydroxyapatite and anhydrous dicalcium phosphate, were much less effective. Calcium metaphosphate produced intermediate results.Moisture content of the soil during the reaction period did not greatly alter subsequent P uptake. The water-soluble sources of phosphorus were affected to the greatest degree.Uptake of P was significantly correlated with the amount of P extracted by NaHCO3 from the treated soils. The highest degree of correlation occurred with ammonium polyphosphate treated soil. A significant negative correlation occurred with calcium metaphosphate. With the exception of the 0.8 bar treatment, moisture tension had little influence on the correlation of P uptake with NaHCO3 extractable-P.
    Print ISSN: 0008-4271
    Electronic ISSN: 1918-1841
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
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